Eocene mafic volcanism in northern Anatolia: its causes and mantle sources in the absence of active subduction

Eocene mafic volcanic rocks occurring in an E-W-trending, curvilinear belt along and north of the Izmir-Ankara-Erzincan suture zone (IAESZ) in northern Anatolia, Turkey, represent a discrete episode of magmatism following a series of early Cenozoic collisions between Eurasia and the Gondwana-derived microcontinents. Based on our new geochronological, geochemical, and isotope data from the Kartepe volcanic units in northwest Anatolia and the extant data in the literature, we evaluate the petrogenetic evolution, mantle melt sources, and possible causes of this Eocene volcanism. The Kartepe volcanic rocks and spatially associated dikes range from basalt and basaltic andesite to trachybasalt and basaltic trachyandesite in composition, and display calc-alkaline and transitional calc-alkaline to tholeiitic geochemical affinities. They are slightly to moderately enriched in large ion lithophile (LILE) and light rare earth elements (LREE) with respect to high-field strength elements (HFSE) and show negative Nb, Ta, and Ti anomalies reminiscent of subduction-influenced magmatic rocks. The analysed rocks have Sr-87/Sr-86((i)) values between 0.70570 and 0.70399, positive E-Nd values between 2.7 and 6.6, and Pb isotope ratios of Pb-206/Pb-204((i))=18.6-18.7, Pb-207/Pb-204((i))=15.6-15.7, and Pb-208/Pb-204((i))=38.7-39.1. The Ar-40/Ar-39 cooling ages of 52.7 +/- 0.5and 41.7 +/- 0.3Ma obtained from basaltic andesite and basalt samples indicate middle to late Eocene timing of this volcanic episode in northwest Anatolia. Calculated two-stage Nd depleted mantle model (T-DM) ages of the Eocene mafic lavas range from 0.6 to 0.3Ga, falling between the T-DM ages of the K-enriched subcontinental lithospheric mantle of the Sakarya Continent (1.0-0.9Ga) to the north, and the young depleted mantle beneath central Western Anatolia (0.4-0.25Ga) to the south. These geochemical and isotopic features collectively point to the interaction of melts derived from a sublithospheric, MORB-like mantle and a subduction-metasomatized, subcontinental lithospheric mantle during the evolution of the Eocene mafic volcanism. We infer triggering of partial melting by asthenospheric upwelling beneath the suture zone in the absence of active subduction in the Northern Neotethys. The geochemical signature of the volcanic rocks changed from subduction- and collision-related to intra-plate affinities through time, indicating an increased asthenospheric melt input in the later stages of Eocene volcanism, accompanied by extensional deformation and rifting.